| 辽西温杖子金矿床成矿特征研究 |
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| 引用本文： | 王丹丽,王恩德.辽西温杖子金矿床成矿特征研究[J].黄金地质,1995,1(4):32-37. |
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| 作者姓名： | 王丹丽 王恩德 |
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| 作者单位： | 沈阳黄金学院 |
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| 摘 要： | 温杖子金矿床位于燕山台褶带辽西断褶束与山海关台拱交接带内，受深大断裂和岩浆活动的控制，形成于中低温条件，成矿溶液以岩浆水为主，并有大气降水混合。围岩蚀变表明与深部岩浆侵入作用有关。研究确定其成因类型为岩浆热液型金矿。
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| 关 键 词： | 金矿床 成矿特征 岩浆热液型 |
A STUDY ON METALLOGENIC FEATURES OF WENZHANGZI GOLD DEPOSIT,WESTERN LIAONING |
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| Wang DanliWang Ende.A STUDY ON METALLOGENIC FEATURES OF WENZHANGZI GOLD DEPOSIT,WESTERN LIAONING[J].Gold Geology,1995,1(4):32-37. |
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| Authors: | Wang DanliWang Ende |
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| Abstract: | Wenzhangzi gold deposit is situated in the contact zone between the Liaoxi platform-subsidence and the Shanhaiguan platform-uplift in Yanshanian folding zone.It is controlled by deep fracturel structures and volcanemagmatic activites.Its mineralizing temprature is low-moderate,the mineralizing fluid is mainly magmatic water and contains atmospheric water. The wallrock alteration shows gold deposit is related the deep magmatic instrusion.It is considered as a magmatic hydrothermal type gold deposit based on the research results. |
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| Keywords: | Liaoning gold deposit metallogenic feature magmatic hydrothermal type gold deposit |
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